• DOI:10.1038/nature19085
• Corpus ID: 4450936

Postglacial viability and colonization in North America’s ice-free corridor

@article{Pedersen2016PostglacialVA,
  title={Postglacial viability and colonization in North America’s ice-free corridor},
  author={Mikkel Winther Pedersen and Anthony Ruter and Charles Earl Schweger and Harvey Friebe and Richard A. Staff and Kristian Kjellerup Kjeldsen and Marie Lisandra Zepeda Mendoza and Alwynne B Beaudoin and Cynthia Zutter and Nicolaj Krog Larsen and Ben A. Potter and Rasmus Nielsen and Rebecca A. Rainville and Ludovic Orlando and David J. Meltzer and Kurt H. Kj{\ae}r and Eske Willerslev},
  journal={Nature},
  year={2016},
  volume={537},
  pages={45-49}
}

• M. W. Pedersen, A. Ruter, +14 authors E. Willerslev
• Published 1 September 2016
• Environmental Science, Geography
• Nature

During the Last Glacial Maximum, continental ice sheets isolated Beringia (northeast Siberia and northwest North America) from unglaciated North America. By around 15 to 14 thousand calibrated radiocarbon years before present (cal. kyr bp), glacial retreat opened an approximately 1,500-km-long corridor between the ice sheets. It remains unclear when plants and animals colonized this corridor and it became biologically viable for human migration. We obtained radiocarbon dates, pollen, macrofossils and metagenomic DNA from lake sediment cores in a bottleneck portion of the corridor. We find evidence of steppe vegetation, bison and mammoth by approximately 12.6 cal. kyr bp, followed by open forest, with evidence of moose and elk at about 11.5 cal. kyr bp, and boreal forest approximately 10 cal. kyr bp. Our findings reveal that the first Americans, whether Clovis or earlier groups in unglaciated North America before 12.6 cal. kyr bp, are unlikely to have travelled by this route into the Americas. However, later groups may have used this north–south passageway.